In situ diffusion experiments in bentonite clay have been carried out in th
e probe CHEMLAB, using the radioactive tracers Co-57, Sr-85 and Cs-134. The
measured diffusion profiles for the radionuclides are in good agreement wi
th predicted profiles obtained from modelling based on apparent diffusiviti
es and sorption coefficients obtained in laboratory experiments with corres
ponding clay density and ground water composition.